Soil Data Explorer - LISMAS

Official Series Description

Lab Data Summary

Aggregate lab data for the LISMAS soil series. This aggregation is based on all pedons with a current taxon name of LISMAS, and applied along 1-cm thick depth slices. Solid lines are the slice-wise median, bounded on either side by the interval defined by the slice-wise 5th and 95th percentiles. The median is the value that splits the data in half. Five percent of the data are less than the 5th percentile, and five percent of the data are greater than the 95th percentile. Values along the right hand side y-axis describe the proportion of pedon data that contribute to aggregate values at this depth. For example, a value of "90%" at 25cm means that 90% of the pedons correlated to LISMAS were used in the calculation. Source: KSSL snapshot (updated 2020-03-18). Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

There are insufficient data to create the lab data summary figure.

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the LISMAS soil series. Monthly precipitation (PPT) and potential evapotranspiration (PET) have been estimated from the 50th percentile of gridded values (PRISM 1981-2010) overlapping with the extent of SSURGO map units containing each series as a major component. Monthly PET values were estimated using the method of Thornthwaite (1948). These (and other) climatic parameters are calculated with each SSURGO refresh and provided by the fetchOSD function of the soilDB package. Representative water storage values (“AWC” in the figures) were derived from SSURGO by taking the 50th percentile of profile-total water storage (sum[awc_r * horizon thickness]) for each soil series. Note that this representation of “water storage” is based on the average ability of most plants to extract soil water between 15 bar (“permanent wilting point”) and 1/3 bar (“field capacity”) matric potential. Soil moisture state can be roughly interpreted as “dry” when storage is depleted, “moist” when storage is between 0mm and AWC, and “wet” when there is a surplus. Clearly there are a lot of assumptions baked into this kind of monthly water balance. This is still a work in progress.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the LISMAS series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot (updated 2024-10-24), parsed OSD records (updated 2024-10-23) and snapshot of SC database (updated 2024-10-23).

Select annual climate data summaries for the LISMAS series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data (updated 2024-10-23).

Geomorphic description summaries for the LISMAS series and siblings. Series are sorted according to hierarchical clustering of proportions and relative hydrologic position within an idealized landform (e.g. top to bottom). Most soil series (SSURGO components) are associated with a hillslope position and one or more landform-specific positions: hills, mountain slopes, terraces, and/or flats. Proportions can be interpreted as an aggregate representation of geomorphic membership. The values printed to the left (number of component records) and right (Shannon entropy) of stacked bars can be used to judge the reliability of trends. Small Shannon entropy values suggest relatively consistent geomorphic association, while larger values suggest lack thereof. Source: SSURGO component records (updated 2024-10-23).

Competing Series

Soil series competing with LISMAS share the same family level classification in Soil Taxonomy. Source: parsed OSD records (updated 2024-10-23) and snapshot of the SC database (updated 2024-10-23).

Select annual climate data summaries for the LISMAS series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data (updated 2024-10-23).

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the LISMAS series and competing. Series are sorted according to hierarchical clustering of proportions and relative hydrologic position within an idealized landform (e.g. top to bottom). Proportions can be interpreted as an aggregate representation of geomorphic membership. Most soil series (SSURGO components) are associated with a hillslope position and one or more landform-specific positions: hills, mountain slopes, terraces, and/or flats. The values printed to the left (number of component records) and right (Shannon entropy) of stacked bars can be used to judge the reliability of trends. Shannon entropy values close to 0 represent soil series with relatively consistent geomorphic association, while values close to 1 suggest lack thereof. Source: SSURGO component records (updated 2024-10-23).

There are insufficient data to create the 2D hillslope position figure.

There are insufficient data to create the 3D hills figure.

There are insufficient data to create the 3D mountains figure.

There are insufficient data to create the 3D terrace figure.

There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with LISMAS, arranged according to family differentiae. Hovering over a series name will print full classification and a small sketch from the OSD. Source: snapshot of SC database (updated 2024-10-23).

Block Diagrams

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

1. KS-2012-01-23-01 | Finney County - November 1965

   Typical cross section of the Pawnee River drainage basin (Soil Survey of Finney County, Kansas; 1965).

2. SD-2012-03-15-45 | Hand County - April 1963

   A typical cross section of the southwestern part of the county (Soil Survey of Hand County, SD; 1963).

3. SD-2012-03-15-47 | Harding County - December 1988

   Pattern of soils and parent material in the Lismas-Winler association (Soil Survey of Harding County, SD; 1988).

Map Units

Map units containing LISMAS as a major component. Limited to 250 records.

Map Unit Name	Symbol	Map Unit Area (ac)	Map Unit Key	National Map Unit Symbol	Soil Survey Area	Publication Date	Map Scale
Lismas clay loam	Lw	938	94848	35pm	co099	1963	1:15840
Lismas-Shale outcrop complex	Lx	276	94849	35pn	co099	1963	1:15840
Yoder-Truckton-Lismas complex	Yt	20205	95353	366x	co624	1963	1:20000
Terry-Lismas complex	Tc	14973	95332	3667	co624	1963	1:20000
Lismas clay	Lc	1852	95302	3658	co624	1963	1:20000
Lismas clay, eroded	Lc2	1811	95303	3659	co624	1963	1:20000
Terry-Lismas complex, severely eroded	Tc3	850	95333	3668	co624	1963	1:20000
Pierre-Lismas clays, saline-Alkali	Pk	23874	345500	clj5	mt103	1961	1:20000
Pierre-Lismas clays	Pc	12489	345499	clj4	mt103	1961	1:20000
Lismas-Pierre clays, saline-Alkali	Ld	11658	345461	clgx	mt103	1961	1:20000
Lismas-Midway complex	Lf	11045	345462	clgy	mt103	1961	1:20000
Lismas clay	Lc	5788	345460	clgw	mt103	1961	1:20000
Lismas-Shale outcrop complex	Lg	5601	345463	clgz	mt103	1961	1:20000
Pierre-Lismas clays, 15 to 40 percent slopes	Pa	14827	345647	clnx	mt109	1956	1:31680
Lismas clay-Shale outcrop, 20 to 60 percent slopes	La	9584	345634	clnh	mt109	1956	1:31680
Lismas clay, 15 to 35 percent slopes	Ln	111147	345761	clsl	mt111	1966	1:20000
Pierre-Lismas clays, 7 to 15 percent slopes	Pl	25244	345785	cltc	mt111	1966	1:20000
Lismas-Shale outcrop complex	Lc	10796	147386	4ycd	mt602	1963	1:20000
Lismas-Pierre clays	La	2696	147385	4ycc	mt602	1963	1:20000
Pierre-Lismas clays, hilly	PN	55408	346097	cm4f	mt607	1970	1:24000
Lismas-Shale outcrop complex, steep	LM	42476	346043	cm2p	mt607	1970	1:24000
Lismas gravelly clay, hilly	LH	35857	346041	cm2m	mt607	1970	1:24000
Lismas-Shale outcrop complex, rolling	LK	33864	346042	cm2n	mt607	1970	1:24000
Pierre-Lismas clays, rolling	PM	24222	346096	cm4d	mt607	1970	1:24000
Midway-Lismas complex, hilly	MVd	18397	346065	cm3d	mt607	1970	1:24000
Lismas-Vananda clays, undulating	LN	14794	346044	cm2q	mt607	1970	1:24000
Midway-Lismas complex, rolling	MVc	11364	346064	cm3c	mt607	1970	1:24000
Lismas gravelly clay, rolling	LG	10469	346040	cm2l	mt607	1970	1:24000
Lismas clay, undulating	LF	1051	346039	cm2k	mt607	1970	1:24000
Lismas clay, hilly	LO	13533	347090	cn5g	mt611	1971	1:24000
Lismas clay, 10 to 40 percent slopes	LcE	148689	2768041	2rd43	sd019	1970	1:24000
Lismas clay, 12 to 45 percent slopes, stony	St	9704	353245	cvl0	sd019	1970	1:24000
Lismas-Pierre clays, 3 to 18 percent slopes	LeD	7229	353193	cvjb	sd019	1970	1:24000
Cabbart-Lismas complex, 6 to 18 percent slopes	CbD	2979	3333641	2zj5b	sd019	1970	1:24000
Lismas-Shale outcrop complex, 25 to 50 percent slopes	Te	2722	353248	cvl3	sd019	1970	1:24000
Lismas, moist-Badland, shale complex, 25 to 50 percent slopes	P208F	47	2668888	2rvdp	sd019	1970	1:24000
Lismas-Winler clays, 6 to 25 percent slopes	LkD	13534	355764	2tvt4	sd063	1984	1:24000
Winler-Lismas clays, 2 to 15 percent slopes	WsC	12851	355816	2y6dm	sd063	1984	1:24000
Lismas-Hisle complex, 6 to 25 percent slopes	LhD	3265	355763	cy67	sd063	1984	1:24000
Lismas-Rock outcrop complex, 15 to 60 percent slopes	LrF	1936	355765	cy69	sd063	1984	1:24000
Lismas clay, 10 to 40 percent slopes	616E	132	2768052	2rd43	sd081	2007	1:24000
Lismas clay, 10 to 40 percent slopes	LbE	71932	2768059	2rd43	sd600	1974	1:24000
Lismas-Winler clays, 6 to 25 percent slopes	LcD	48185	354325	2tvt4	sd600	1974	1:24000
Winler-Lismas clays, 6 to 15 percent slopes	WlC	5007	355475	cxwy	sd601	1983	1:24000
Pierre-Lismas clays, 15 to 40 percent slopes	PlE	4918	355459	cxwf	sd601	1983	1:24000
Lismas clay, 10 to 40 percent slopes	LbE	4153	2768063	2rd43	sd601	1983	1:24000
Lismas clay, 3 to 30 percent slopes	P206E	3894	2745760	2rvdg	wy011	1978	1:24000
Lismas-Grummit complex, 10 to 30 percent slopes	P210E	1393	2745761	2rxs1	wy011	1978	1:24000
Lismas-Sabatka-Xema complex, 3 to 15 percent slopes	227	149	780141	2wlrm	wy011	1978	1:24000
Lismas clay, 3 to 30 percent slopes	P206E	145	2745986	2rvdg	wy045	1984	1:24000
Lismas-Sabatka-Badland complex, 3 to 45 percent slopes	164	6967	349856	cr1p	wy605	1995	1:24000
Lismas-Mittenbutte, cool-Sabatka complex, 6 to 40 percent slopes	162	2965	349853	cr1l	wy605	1995	1:24000
Lismas-Sabatka-Xema complex, 3 to 15 percent slopes	295	33706	817638	2wlrm	wy705	2003	1:24000
Badland-Lismas complex, 15 to 75 percent slopes	254	23472	817639	2yrxy	wy705	2003	1:24000
Lismas-Sabatka-Badland complex, 3 to 45 percent slopes	164	8508	817546	wfqg	wy705	2003	1:24000
Lismas-Mittenbutte, cool-Sabatka complex, 6 to 40 percent slopes	162	61	817545	wfqf	wy705	2003	1:24000

Map of Series Extent

Approximate geographic distribution of the LISMAS soil series. To learn more about how this distribution was mapped, or to compare this soil series extent to others, use the Series Extent Explorer (SEE) application. Source: generalization of SSURGO geometry (updated 2024-10-30).